|Extrusive igneous rock|
|Primary||nepheline, sodalite, hauyne, leucite, analcite, sanidine, anorthoclase|
|Secondary||biotite, amphibole, pyroxene, olivine|
Phonolite is an uncommon extrusive igneous rock, volcanic rock, of intermediate chemical composition between felsic and mafic, with texture ranging from aphanitic (fine-grain) to porphyritic (mixed fine- and coarse-grain).
The name phonolite comes from the Greek meaning "sounding stone" because of the metallic sound it produces if an unfractured plate is hit; hence the English name clinkstone.
|This section does not cite any sources. (July 2013)|
Unusually, phonolite forms from magma with a relatively low silica content, generated by low degrees of partial melting (less than 10%) of highly aluminous rocks of the lower crust such as tonalite, monzonite and metamorphic rocks. Melting of such rocks to a very low degree promotes the liberation of aluminium, potassium, sodium and calcium via melting of feldspar, with some involvement of mafic minerals. Because the rock is silica undersaturated, it has no quartz or other silica crystals, and is dominated by low-silica feldspathoid minerals more than feldspar minerals.
A few geological processes and tectonic events can melt the necessary precursor rocks to form phonolite. These include intracontinental hotspot volcanism, such as may form above mantle plumes covered by thick continental crust. A-type granites and alkaline igneous provinces usually occur alongside phonolites. Low-degree partial melting of underplates of granitic material in collisional orogenic belts may also produce phonolites.
Mineralogy and Petrology
Mineral assemblages in phonolite occurrences are usually abundant feldspathoids (nepheline, sodalite, hauyne, leucite and analcite) and alkali feldspar (sanidine, anorthoclase or orthoclase), and rare sodic plagioclase. Biotite, sodium-rich amphiboles and pyroxenes along with iron-rich olivine are common minor minerals. Accessory phases include titanite, apatite, corundum, zircon, magnetite and ilmenite.
Nepheline syenites and phonolites occur widely distributed throughout the world in Canada, Norway, Greenland, Sweden, the Ural Mountains, the Pyrenees, Italy, Eifel and Kaiserstuhl in Germany, Brazil, the Transvaal region, the Magnet Cove igneous complex of Arkansas, the Beemerville Complex of New Jersey, as well as on oceanic islands such as the Canary Islands.
- Devils Tower, Wyoming, USA, a striking example of columnar jointed phonolite
- Dunedin, New Zealand
- Bořeň, northwestern Czech Republic
- Hoodoo Mountain, northwestern British Columbia, Canada
- Jebel Nefusa, Libya
- Teide, a stratovolcano on the island of Tenerife
- Mont Gerbier de Jonc South East France
- The phonolitic lava lake in Mount Erebus, Ross Island, Antarctica
- Cripple Creek & Victor Gold Mine phonolite pipe
- Montiferru, Sardinia
Phonolites can be of interest as dimension stone or as aggregate for gravels.
Rarely, economically mineralised phonolite-nepheline syenite alkaline complexes can be associated with rare earth mineralisation, uranium mineralisation and phosphates, such as at Phalaborwa, South Africa.
Phonolites can be separated into slabs of appropriate dimensions to be used as roofing tiles in place of roofing slate. One such occurrence is in the French Massif Central region such as the Haute Loire département.
- Ridley, W.I., 2012, Petrology of Igneous Rocks, Volcanogenic Massive Sulfide Occurrence Model, USGS Scientific Report 2010-5070-C, Chapter 15
- Blatt, Harvey and Robert J. Tracy, Petrology, Freeman, 2nd ed. 1996, p. 52, ISBN 0-7167-2438-3
- Woolley, A.R., 1995. Alkaline rocks and carbonatites of the world., Geological Society of London.
- Eby, G. N., 2012, The Beemerville alkaline complex, northern New Jersey, in Harper, J. A., ed., Journey along the Taconic unconformity, northeastern Pennsylvania, New Jersey, and southeastern New York: Guidebook, 77th Annual Field Conference of Pennsylvania Geologists, Shawnee on Delaware, PA, p. 85-91.
- S. E. Bryana, R. A. F. Cas, and J. Mart, 1998. Lithic breccias in intermediate volume phonolitic ignimbrites, Tenerife (Canary Islands): constraints on pyroclastic flow depositional processes, Journal of Volcanology and Geothermal Research, v81, May 1998, Pages 269-296.
- Bassett, W. A. (October 1961). "Potassium-Argon Age of Devils Tower, Wyoming". Science 134 (3487): 1373–1373. Bibcode:1961Sci...134.1373B. doi:10.1126/science.134.3487.1373. ISSN 0036-8075.
- Marshall, Patrick, 'The occurrence of a mineral hitherto unknown in the phonolites of Dunedin, New Zealand', 1929.
- Bausch, W.M., The central part of the Jebel Nefusa volcano (Libya) survey map, age relationship and preliminary results, International Journal of Earth Sciences, 1978, pp 389-400 ISSN 1437-3262
- Ablay, G.J. et al. (1998) Basanite–Phonolite Lineages of the Teide–Pico Viejo Volcanic Complex, Tenerife, Canary Islands, Journal of Petrology, volume 39 number 5 pages 905-936 PDF - retrieved 2010-02-24
- Affolter, J., 2002 Provenance des silex préhistoriques du Jura et des régions limitrophes., Archéologie neuchâteloise, 28
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